You should have seen from the video that the stability of the carbonates towards heat increased as we went down the group. This is linked to the size of the ion which is illustrated in the table below:
| Cation | Ionic radius (nm) | Time to cloudiness (s) | Degree of cloudiness | Decomposition Temperature (K) |
| Mg2+ | 0.072 | 27 | high | 813 |
| Ca2+ | 0.100 | 80 | medium | 1173 |
| Sr2+ | 0.113 | 120 | slight | 1563 |
| Ba2+ | 0.136 | - | very slight | 1573 |
The explanation behind this is that the smaller group 2 cations have a greater polarizing effect on the carbonate ion, causing it to decompose to a metal oxide and carbon dioxide gas more readily. The equations are all very similar:
|
MgCO3(s) ⇒ MgO(s) + CO2(g) |
CaCO3(s) ⇒ CaO(s) + CO2(g) |
|
SrCO3(s) ⇒ SrO(s) + CO2(g) |
BaCO3(s) ⇒ BaO(s) + CO2(g) |
The polarising effect is much less with a 1+ ion. Most group1 carbonates do not decompose under normal heating. Only lithium carbonate (with the smallest positive ion) decomposes in the same way as the group 2 carbonates.